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Evolution of late Palaeozoic shearing in the Cobequid Highlands: constraints on the fragmentation of the Appalachian orogen in Nova Scotia along intra-continental shear zones

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posted on 2020-04-16, 14:43 authored by David J. W. Piper, Georgia Pe-Piper

Figure S3. Proposed trace of the Lynn Mountain Fault.

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Evolution of late Palaeozoic shearing in the Cobequid Highlands: constraints on the fragmentation of the Appalachian orogen in Nova Scotia along intra-continental shear zones

Geological Society, London, Special Publications

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Geology not elsewhere classified

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Cobequid Highlands Palaeozoic shearing intra-continental shear zones Figure S 3.Lynn Mountain Fault Appalachian orogen trace fragmentation Nova Scotia evolution constraint Geology

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